Process-diagnostic patterns of chlorobiphenyl congeners in two radiochronologically characterized sediment cores from the northern Baffin Bay

Citation
O. Gustafsson et al., Process-diagnostic patterns of chlorobiphenyl congeners in two radiochronologically characterized sediment cores from the northern Baffin Bay, CHEMOSPHERE, 45(6-7), 2001, pp. 759-766
Citations number
22
Categorie Soggetti
Environment/Ecology
Journal title
CHEMOSPHERE
ISSN journal
00456535 → ACNP
Volume
45
Issue
6-7
Year of publication
2001
Pages
759 - 766
Database
ISI
SICI code
0045-6535(200111)45:6-7<759:PPOCCI>2.0.ZU;2-C
Abstract
Polychlorinated biphenyl (PCB) patterns were interpreted in two radioisotop ically constrained sediment cores from the Arctic ocean in order to seek cl ues about their large-scale environmental fates. Low but clearly measurable fluxes of individual PCB congeners were observed in deeper layer sediments , corresponding to the past 170 years, in a single dated core from the Baff in Bay shelf. Fluxes of the dominant individual congeners in the surface se diments were 20-100 mug m(-2) d(-1). Combining these data with the sediment data from the Arctic Monitoring and Assessment Program, it appears that th e PCB distribution in Arctic surface sediments is governed by the organic c arbon (OC) content of the sediments. The historical development of the PCB congener fingerprint suggests that the modern sediments are enriched in med ium-chlorinated congeners, implying that there are at least two significant , but distinctly different, sink processes acting on the PCB pool. The rela tive abundance of light-to-heavy congeners, in mid-shelf marine sediments o f similar ages, between 40 degreesN and 76 degreesN latitude suggests a nor thward dilution of PCBs which is stronger attenuated for heavier congeners, consistent with a temperature-driven global fractionation process. The sig nificant presence of PCB in historical archives pre-dating the organochlori ne society, as observed in this and several previous studies, awaits a full er explanation. (C) 2001 Elsevier Science Ltd. All rights reserved.